Climate 101

Graphic of the electromagnetic spectrum comparing wave size to objects

Basics of Radiative Forcing

The temperature of the surface of the earth is essentially determined by two things: the amount of energy coming in from the sun and the amount of energy emitted out into space by the Earth and its atmosphere. (Interestingly, that hot molten core under the earth’s crust plays very little…
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Common Climate Units

Climate change units can be confusing. Letters and numbers. Uppercase, lowercase, subscript. How to make sense of a weird agglomeration like GtCO₂e? As long as the article is well written and internally consistent, you may be able to glide right over them and still get the gist. But if you…
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More GWP*

If you haven’t seen them already, you may want to read this post about GWP and this post about GWP* first. So should we abandon GWP for methane emissions and begin using GWP* instead? That’s what many advocates for beef, dairy, and sheep have been arguing. It’s even found support…
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Cow

What about GWP*?

If you haven’t read them already, you may want to read this post about GWP and this post about GTP first. Both Global Warming Potential (GWP) and Global Temperature Potential (GTP) were designed for a relatively straightforward goal: to enable the comparison between different greenhouse gases. For example, if someone…
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